LIU Shuo, LIU Qingshan, ZHANG Junzi, DU Yangyang, WANG Candanting, LIANG Hefeng
Liuheying-Daxinzhuang structural belts are second-level oil-bearing structural belts located at the southwestern end of the western zone in Langgu Sag, with low degree of exploration. Due to its complex structure and sparse survey grid, the hydrocarbon accumulation regularities remain unclear. Based on the data of well-seismic combination, actually drilled geology and analytic test, the hydrocarbon accumulation conditions and exploration potential are deeply analyzed. The results are obtained in four aspects. First, The Es3l dark mudstone is the dominant source rock beds and has good oil source conditions with a large thickness of 600-1 600 m, high organic matter abundance of TOC 0.64%-1.03%, and main kerogen type Ⅱ₂-Ⅲ. Second, As a whole, Es3 reservoirs are dominated by medium-high porosity and low permeability, with the best physical properties in Es3m of Daxinzhuang arched structural belt, and the reservoir-cap rock assemblage in Es3 is superior. Third, The structural belts are clamped between the two large oil-generating troughs of western Gu′an and southern Liuheying, the oil and gas enrichment is jointly controlled by the nose-like structural trap, the turbidite sand body distribution, and the dual effects of oil source fault transport and later tectonic uplift, forming the down generated up stored and side generated lateral stored reservoir-forming patterns. Fourth, two reservoir-forming patterns of ridge-type and toothbrush-shaped structures were constructed to reveal the banded enrichment regularity of oil and gas along the structural high parts and faults. G 8 trap and No.2 trap in northern L 1 were selected as the most favorable targets from 49 traps, with the total quantity of oil resources of over 500×104 t and natural gas of nearly 40×108 m3 predicted. The results provide theoretical guidance and technical support for the subsequent research and exploration of oil-bearing traps in the complex structural zones of Langgu Sag.